Preprints
https://doi.org/10.5194/angeo-2024-29
https://doi.org/10.5194/angeo-2024-29
08 Jan 2025
 | 08 Jan 2025
Status: this preprint is currently under review for the journal ANGEO.

Ozone decrease observed in the upper atmosphere following the May 11th 2024 Mother’s day solar storm

Alexandre Winant, Viviane Pierrard, and Edith Botek

Abstract. On May 11th 2024, a succession of coronal mass ejections that merged together struck the Earth and induced large scale perturbations in the magnetosphere. During this event, satellite observations showed a large solar energetic proton (SEP) event associated to an extreme geomagnetic storm. At the same time, satellite observations of atmospheric ozone have been performed by AURA/MLS. In this work, we present the first observations of the effect of the storm of May and the following SEP of June 8th on ozone concentration throughout the atmosphere. Observations of the MLS show that the event of May lead to stronger depletion of O3 in the upper part of the atmosphere than in June. This difference is explained by the type of particle precipitation that occurred during the two events, with both protons and electrons in May and only protons in June. Neither event caused ozone depletion in the stratosphere while strong decreases are observed in the mesosphere. In May, mesospheric ozone depletion is observed during 18 days and reaches a maximum of 60 %. In addition, the storm of May also caused a noticeable decrease in ozone concentration (up to 20 %) at altitudes above 90 km.

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Alexandre Winant, Viviane Pierrard, and Edith Botek

Status: open (until 19 Feb 2025)

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Alexandre Winant, Viviane Pierrard, and Edith Botek
Alexandre Winant, Viviane Pierrard, and Edith Botek

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Short summary
The intense solar storm of May 11th 2024 struck the Earth causing a large influx of solar protons into the atmosphere. It also caused the largest geomagnetic disturbances observed in the past 20 years. Space particles when they penetrate the atmosphere influence its chemistry. In this work we use satellite-based observations to study the effect of this major event on atmospheric ozone. We show that ozone in the upper southern polar atmosphere was clearly lost following this event.